Warm and cold events in the Gulf of Guinea, characteristic of the tropical interannual variability,can be generated in several ways. This emerges from a statistical analysis of 200 years ofinterannual variability simulated by a coupled ocean–atmosphere General Circulation Model.The application of a clustering technique to the anomalies of the thermal energy stored in theupper oceanic layers leads to the separation of the events, either warm or cold, into a numberof classes, each of them distinguished by a particular generation scheme. The physical mechanismsinvolved are identified by examining the contributions of the various terms in the mixedlayer tendency equation.Basically, those few classes can be sorted into two larger groups. In one of them, the onsetstage is characterized by an eastward propagation of the anomalies. Atmospheric flows play aleading part in the generation of events within this group. In the second group, thermal energyanomalies are generated in situ in the Gulf of Guinea, and it is mixing that gives the mostimportant contribution to the development of the events.The different classes are related to different seasonal signatures and also to differences in theinfluence of the El Ninˆo-Southern Oscillation (ENSO). While some of the classes are stronglyinfluenced by ENSO, while in others this influence is not significant. This can explain thebarely significant correlations between ENSO and the Atlantic warm events, a feature that thesimulation analyzed here shares with the observations.DOI: 10.1034/j.1600-0870.2002.01316.x